Oct 2026· GRACE/GRACE-FO Science Team Meeting 2026· 0 citations
Abstract
While monthly Level-2 products of GRACE/-FO are widely used as essential climate variables for mass-transport studies, published processing chains and intermediate outputs are often insufficiently documented for transparent diagnostics, method intercomparison, and fully reproducible re-solving. Building on existing uses of the Level-1C concept, we present Hawk Level-1C, an integrated scientific dataset that links calibrated Level-1B observations with monthly Level-2 gravity fields and supports consistent, transparent, traceable, and reproducible mass-change studies with GRACE/GRACE-FO. Specifically, this Level-1C dataset comprises four subsets: (1) K-band range-rate residuals, (2) line-of-sight gravity differences, (3) normal equations, and (4) calibrated accelerometer data. Each subset provides much complementary information beyond conventional Level-2 gravity fields and opens up new scientific applications, making it possible to (1) recover the submonthly gravity signal, (2) monitor rapidly evolving events such as floods and hurricanes, (3) enable accurate land water assimilation/fusion, and (4) perform neutral density modeling related to space weather. This product is provided on a monthly basis, spanning the available mission months from April 2002 to June 2026, to cover both GRACE and GRACE-FO, which will be openly available through Zenodo soon. In addition, we declare that this Level-1C, as well as the companion Level-2 product, is completely reproducible through our open source software and the configuration files provided. In this work, the entire data processing chain from Level-1B to Level-1C and Level-2 is documented. Long term diagnosis and rigorous validation of our Level-1C against other publicly available resources are carried out, which have demonstrated the satisfactory quality of our product. In the end, we showcase how this product helps to explore and exploit the scientific potential of GRACE/GRACE-FO in a manner different from the standard Level-2 product.
The Gravity Recovery and Climate Experiment Follow-On (GRACE-FO), launched in May 2018, provides invaluable information about mass change in the Earth system, continuing the legacy of GRACE. Fundamental requirements for successful mass change recovery are precise orbit determination and inter-satellite ranging, determi...
C. Mccullough, Willy Bertiger, S. Byun et al.· GRACE/GRACE-FO Science Team...· 0 citations
Understanding the nonstationarity of GRACE/GRACE-FO-derived terrestrial water storage anomalies (TWSA) is crucial for interpreting component-scale water storage variability, improving TWSA modeling, and supporting evaluation of land-surface and global hydrological models. However, existing studies lack methods for expl...
H. Pham, Joseph Awange, Sten Claessens et al.· Natural Resources Research· 1 citation
GRACE and GRACE-FO satellite missions measure the spatial and temporal variations in the Earth’s gravity field at a spatial resolution of around 300 kilometers. Unlike most gravity field products available at monthly resolutions, the CNES produces a 10-day Level 2 solution constrained by Satellite Laser Ranging using...
This study directly utilises GRACE Level-1B (L1B) KBR post-fit residuals, provided by the Center for Space Research, as the basis for high-frequency mass change modelling. We showcase the updated methodology and its uncertainty characteristics, demonstrating the potential of KBR post-fit residuals to recover sub-monthl...
M. Cuadrat-Grzybowski, Frederik Jacobs, J. de Teixeira da Encarnacao· GRACE/GRACE-FO Science Team...· 0 citations
Sea-level rise is a key indicator of climate change, increasing the vulnerability of the Mediterranean’s densely populated, socio-economically important coastlines. This study investigates Mediterranean sea-level variability and its physical components over 2005–2025. Multi-mission altimetry products, which retain inte...
Rafailia N. Adam, G. Vergos· Geomatics· 0 citations
Currently available GRACE and GRACE Follow-On (GRACE(-FO)) mascon solutions differ due to variations in parameterization, regularization and land-ocean classification, leading to inconsistencies in regional mass change estimates. To reduce dependence on any single processing strategy, we present the first fused mascon...
Rebecca McGirr, P. Tregoning· GRACE/GRACE-FO Science Team...· 0 citations
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